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  June 09, 2008

The Black Disk:  A Different Approach to Measuring Water Clarity

Excerpted from IF WATER CLARITY IS THE ISSUE, THEN WHY NOT MEASURE IT?*
Complete Article available at:  http://www.nwqmc.org/NWQMC-Proceedings/Papers-Alphabetical%20by%20First%20Name/David%20Smith2.pdf
D.G. Smith,
Department of Environmental Protection,
Bureau of Water Supply

465 Columbus Avenue,
Valhalla, New York, NY 10595
and

R.J. Davies-Colley,
National Institute of Water and Atmospheric Research Ltd. (NIWA)
P.O. Box 11-115,
Hamilton, New Zealand

* Poster paper presented at the National Water Quality Monitoring Council Annual Conference, Madison, Wisconsin, May 2002. Proceedings available at www.nwqmc.org.

Introduction

Suspended sediment causes many adverse aquatic impacts, including:
• transport of other pollutants
• benthic smothering
• costly treatment of water supplies

Often, the worst impact is optical—caused by decreased light transmission through water. This has two main effects:
• reduced light penetration for photosynthesis
• reduced visual range of sighted organisms, including people  

Unfortunately, concepts of suspended sediment concentration (SSC), nephelometric turbidity, and visual water clarity are poorly understood.

This paper is based on a recent review of the topic (Davies-Colley & Smith, 2001) and emphasizes the use of visual water clarity measurement.

Visual Water Clarity  

Visual clarity has been traditionally measured in lakes using a Secchi disc.  But the conventional Secchi disc measurement has several problems:
• as a vertical measurement, it needs relatively deep water
• it has no accepted protocol
• it is dependent on lighting conditions  

The All-Black Disc

A better measure of visual clarity is obtained using an all-black disc viewed horizontally.  A horizontal black disc measurement has several advantages:
• it can be performed in very shallow waters
• it is independent of lighting conditions (being black, its orientation relative to the sun is unimportant)
• it is very simply related to beam attenuation coefficient (a fundamental optical property)
• it can be used in lentic situations (lakes and ponds) as well as moving water

Turbidity

Turbidity (water cloudiness) is usually measured in the laboratory (units: NTU) and is often, uncritically, taken to be equivalent to visual clarity.  There are several problems with turbidity measurement, for instance:
• different instruments may produce different numbers
• it is an arbitrary measurement, usually measured relative to a formazin standard
• it is not a 'proper' scientific measure
• turbidity is not uniquely related to visual clarity or SSC

We discourage its use as a general environmental measurement.

Inter-relationships Between Turbidity, Suspended Sediment Concentration, and Visual Clarity

These three measurements are only broadly correlated, although the optical variables (visual clarity and turbidity) are more closely related to each other than SSC. However, the relationships are inadequate for general use and for useful predictive purposes. Also, waters at different sites having the same turbidity can have widely different visual clarities.  

         

Mutual relationships in 97 New Zealand rivers at base flow (Hach 2100A nephelometer).

Sometimes useful, close relationships are found in waters having particles of similar optical character—these are usually site-specific.  

 

SSC is not relevant when the impacts of concern are optical.  Turbidity is not immediately relevant in environmental studies because it needs to be calibrated to visual clarity at different sites.  Visual clarity has most environmental relevance because it is a direct measure of an optical attribute that strongly affects aquatic habitat and human uses of waters.

Visual clarity measurement is highly suitable for general optical environmental standards, unlike SSC and turbidity.

Conclusions

If the effect of interest of suspended sediment is optical, and related to visual sighting range, then measure visual clarity using the horizontal black disc technique.

Visual clarity:
•     is a true scientific measurement
     has immediate environmental relevance
•     is readily understood
•     is not particularly subjective
     can be measured with better precision than SSC and turbidity
•     is more relevant than SSC and turbidity
•     should be used in environmental standards dealing with water optics
 

REFERENCES  

Davies-Colley, R. J. and D. G Smith, 2001.  Turbidity, Suspended Sediment, and Water Clarity: A Review. Journal of the American Water Resources Association 37: 1085-1101.

 

Attribute

Cost

Precision
(typical standard error)

Sample size & storage

 

Continuous monitoring?

Environmental relevance

Suspended sediment concentration (SSC)

$23/sample

 

10%

 

100 mg residue*

(sample fairly stable if chilled, dark)

No (needs laboratory)

Relevant to sediment yields and benthic effects of sedimentation Less relevant to optical impacts.

 

Turbidity

 

$5/sample

10%

< 100 mL
(unstable-keep chilled, dark, and measure in less than 24 hours)

Yes

(turbidity monitors)

Measurement is relative to arbitrary standards. Requires calibration (e.g., to suspended solids Indirectly relevant to solids or visual clarity).

 

Visual clarity, alternatively, beam attenuation coefficient)

$4/observation

4%

Not applicable (usually done in situ)

  Yes, as beam transmittance

  Relevant to aesthetic quality of water and habitat for sighted aquatic animals.

 * Requires 10 liter sample at 10 g m-3 for high precision. Volumes may get prohibitively large in clearer waters.

ADDITIONAL RESOURCES ON BLACK DISKS

Theory and how to build the disk

"Measuring Visibility in Moving Waters"     http://depts.washington.edu/cssuw/Publications/FactSheets/secchic.pdf


For more information on the Great American Secchi Dip-In, contact us at: DipIn@kent.edu or write

Great North American Secchi Dip-In
Department of Biological Sciences
Kent State University
Kent OH 44242